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Spatiotemporal heterogeneity of magnetic enhancement mechanisms in aeolian deposits on the southern Tibetan Plateau: Implications for paleoclimatic reconstruction in mountain- basin systems
WANG Haoyu, YANG Junhuai, QU Wenxi, WANG Linkai, ZHANG Canyi, LIU Xin, TANG Jinmeng, GAO Fuyuan, CHEN Zixuan, WANG Shuyuan, FAN Yijiao, WU Duo
地理学报(英文版), 2026, 36(1): 177-198.   DOI: 10.1007/s11442-026-2443-7

Figure 1 Geographical and climatic context of the study area. (a) Locations of the investigated sections (SGX, HZ, MR sections, green pluses) and referenced aeolian sections from the Ili basin (green dots), Chinese Loess Plateau (blue dots), and desert peripheries (orange dots). Major atmospheric circulation systems are also shown: Indian summer monsoon (ISM), mid-latitude westerlies (MLW), East Asian summer monsoon (EASM), and East Asian winter monsoon (EAWM). (b-d) Mean monthly temperature and precipitation data for the three investigated sections, sourced from WorldClim (https://worldclim.org/data/index.html).
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